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Genesis and Taphonomy of the Archaeological Layers of Pedra

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Quaternaire Revue de l'Association française pour l'étude du Quaternaire vol. 29/3 | 2018 Volume 29 Numéro 3 Genesis and taphonomy of the archaeological layers of Pedra Furada rock-shelter, Brazil Genèse et taphonomie des niveaux archéologiques de l’abri de la Pedra Furada, Brésil Fabio Parenti, Alan Cannell, Evelyne Debard, Martine Faure et Mercedes Okumura Édition électronique URL : http://journals.openedition.org/quaternaire/10313 ISSN : 1965-0795 Éditeur Association française pour l’étude du quaternaire Édition imprimée Date de publication : 1 septembre 2018 Pagination : 255-269 ISSN : 1142-2904 Référence électronique Fabio Parenti, Alan Cannell, Evelyne Debard, Martine Faure et Mercedes Okumura, « Genesis and taphonomy of the archaeological layers of Pedra Furada rock-shelter, Brazil », Quaternaire [En ligne], vol. 29/3 | 2018, mis en ligne le 01 septembre 2020, consulté le 10 janvier 2019. URL : http:// journals.openedition.org/quaternaire/10313 © Tous droits réservés Quaternaire, 29, (3), 2018, p. 255-269 255 GENESIS AND TAPHONOMY OF THE ARCHAEOLOGICAL LAYERS OF PEDRA FURADA ROCK-SHELTER, BRAZIL n Fabio PARENTI1,2, Alan CANNELL2, Evelyne DEBARD3, Martine FAURE4 & Mercedes OKUMURA5 Pour Claude, un Maître et un ami. ABSTRACT New sedimentological and taphonomic analyses of a preserved bulk of Pedra Furada rock-shelter characterize the mixed origin of the illing, both from the sandstone wall and from the uppermost conglomerate layer. Statistical analysis of quantitative and qualitative data on waterfalls and archaeological assemblage, both dated from the Upper Pleistocene and Holocene, demonstrated no causal relationship among Eastern waterfall talus, lithic tools and archaeological structures. Technical similarities have been reported between extant monkeys unintentional laking by-products and the lithic toolkit from the previous archaeological excavations. Comparison between present monkey’s hammerstones and the quartz elements recorded in archaeological structures point to a clear anthropic selection in the making of archaeological structures in the site, regardless of any association with charcoals. Because of the similarities between the present monkey stone-tools and the (supposed) human tool-kit, the inclusion of both human and primate archaeologies in an interdisciplinary research program is needed to clarify the nature of pre-Clovis presence in South America. Keywords: Sedimentology, Upper Pleistocene, Pedra Furada, statistics, lithic tools, archaeological structures, Platyrrhines RÉSUMÉ GENÈSE ET TAPHONOMIE DES NIVEAUX ARCHÉOLOGIQUES DE L’ABRI DE LA PEDRA FURADA, BRÉSIL Les nouvelles recherches sédimentologiques et taphonomiques conduites sur le bloc-témoin de l’abri de la Pedra Furada mettent en évidence la double origine du remplissage, provenant de la paroi gréseuse et des niveaux conglomératiques supérieurs. Les données quantitatives et qualitatives concernant les chutes d’eau et le contenu archéologique du site, tant dans les niveaux pléistocènes que holocènes, démontrent l’absence de relation de causalité entre le talus de la chute d’eau orientale, l’outillage lithique et les structures archéologiques. Des similaritées technologiques ont été observées et comparées entre les produits lithiques non intentionnels des singes actuels et ceux provenants des anciennes fouilles. La comparaison entre la masse des percuteurs utilisés par les singes actuels et celle des galets de quartz utilisés, retrouvés dans les structures archéologiques, indique une évidente sélection d’origine anthropique dans la disposition des structures, avec ou sans restes de combustion. Du fait de la similarité entre l’outillage des singes actuels et celui (supposé) humain dans le passé, une double archéologie anthropique et simienne est le seul moyen d’éclaircir la vraie nature de la présence humaine pré-Clovis en Amérique du Sud. Mots-clés : Sédimentologie, Pléistocène supérieur, Pedra Furada, statistiques, outillage lithique, structures archéologiques, Platyrrhiniens 1 - INTRODUCTION Meltzer et al., 1994; Borrero, 1995; Guidon et al., 1996; Michab et al., 1998; Parenti, 2001). Since 1974 the entire For more than twenty years, the region of the Serra Serra da Capivara National Park and its surroundings da Capivara National Park, located in Piauí state, have been intensively studied from a multidisciplinary Northeastern Brazil, has been the focus of a harsh approach, recording - among others - several sites debate on pre-Clovis evidence in South America, mainly presenting Pleistocene palaeontological (Guérin & Faure, centered on the evidence of the reference site, the 2008, 2014) and archaeological remains (Lourdeau & Boqueirão da Pedra Furada (BPF) rock-shelter (main Pagli, 2014). In particular, since 2008, research under the references: Guidon & Delibrias, 1986; Butzer, 1988; direction of Eric Boëda has been conducted with the aims 1 Departamento de Antropologia, Universidade Federal do Paraná, PR, BR-80060-150 Curitiba. Email: [email protected] 2 Istituto Italiano di Paleontologia Umana, IT-03012 Anagni. Email: [email protected] 3 Université de Lyon, UCBL, ENSL, CNRS, LGL-TPE, FR-69622 Villeurbanne. Email: [email protected] 4 Université Lumière - Lyon 2, UFR Temps et Territoires; and Université de Lyon, UCBL, ENSL, CNRS, LGL-TPE, FR-69622 Villeurbanne. Fundação Museu do Homem Americano, São Raimundo Nonato (Piauí, Brasil). Email: [email protected] 5 Laboratório de Estudos Evolutivos Humanos, Departamento de Genética e Biologia Evolutiva, Instituto de Biociências, Universidade de São Paulo, Rua do Matão, 277, Cidade Universitária, Butantã, SP, BR-05508-090. Email: [email protected] Manuscrit reçu le 31/10/2017, accepté le 26/02/2018 256 of replicating and reining the data obtained at the BPF site there has recently been the discovery of platyrrhine and discovering new evidence of Pleistocene occupations monkeys as battering and laking agents in the Brazilian in the region (Lahaye et al., 2013; Boëda et al., 2014, lowlands (Profitt et al., 2016). 2016). Although the results obtained at BPF, excavated In the background of the criticisms advanced about between 1978 and 1988, have been exhaustively published the Pleistocene sites in Serra da Capivara region, we since 2001 (Parenti, 2001; Santos et al., 2003; Valladas et are well aware that the core issue is the taphonomic and al., 2003; Chaves et al., 2006), many recent publications contextual analysis of each speciic set of evidence. For a do not even consider the abovementioned detailed data, long time the focus of research has been the chronology preferring to focus their critiques on a generic and and classiication of archaeological remains, without conjectural set of taphonomic and technological remarks or paying due attention to the formation processes of even, naively, ignoring the existence of the site itself when deposits and evaluation of alternative explanations. In considering the issue of a pre-Paleoindian occupation in this sense, a irst step was made in the book on BPF, South America (Bueno et al, 2013; Vialou et al., 2017). when considering gravity as a possible agent for cobbles Meanwhile, several research programs have focused fracture (Parenti, 2001, ch. 5). However, at the time on complementary aspects of the main debated issue, i.e. of this study (1988-1992) a detailed sedimentological the hypothesis of a human colonization of the Americas analysis was still missing and therefore a well-founded during the Pleistocene; among these are: 1) a huge statistical analysis could not be carried out. array of genetic studies that aim at tracing the origin of In this article we present four new sets of data concerning population stock(s) and the timing of their spread(s), the formation processes at BPF: 1) a sedimentological generally admitting a irst peopling event not older description of the illing, partially based on the 1987- than 20 ka BP (Zegura et al., 2004) 2) a model of two 1988 excavations but mainly on unpublished data from settlement waves based on cranial morphology (Hubbe a ield campaign conducted in 1996 on the preserved et al., 2014); 3) new archaeologically consistent and bulk in the Eastern sector of the site; 2) a statistical well-dated pre-Clovis sites (McAvoy & McAvoy, 1997; comparison between the natural fracture of quartz cobbles Stanford et al., 2014 ; Dillehay et al., 2015); 4) the role from the base of the western waterfall and the artifacts of Beringia refugia during the Last Glacial Maximum as recovered in the excavations, in order to investigate any cradle of American population waves (Hoffecker et al., gravitational action in the making of the assemblage 2016); 5) a re-birth of the controversial hypothesis of and its relation to the artefacts, manuports or supposed an North-Atlantic Ice-Age coastal entry route in North geofacts; 3) a comparison between the granulometry of America, i.e. the “Solutrean hypothesis” (Stanford & the illing and the composition of some representative Bradley, 2012; Eren et al., 2013). To add to this debate features of Pleistocene units; 4) a synopsis of main Fig. 1: Position of the site (BPF) in relation to the sandstone cuesta and the nearby rock-shelter of Sítio do Meio (SDM) ; image from GoogleEarth. The whitish edge of the cliff is the uppermost outcropping conglomerate layer. Note the thalweg just South of BPF, comprised between elevations 383 and 393. Fig. 1 : Localisation du site (BPF) par rapport à la cuesta gréseuse et à l’abri-sous-roche du Sítio do Meio (SDM) ; image de GoogleEarth. Le
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  • The Distribution of Paleoindian Debitage from the Pliestocene Terrace at the Topper Site: an Evaluation of a Possible Pre-Clovis Occupation (38AL23)

    The Distribution of Paleoindian Debitage from the Pliestocene Terrace at the Topper Site: an Evaluation of a Possible Pre-Clovis Occupation (38AL23)

    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 5-2012 The Distribution of Paleoindian Debitage from the Pliestocene Terrace at the Topper Site: An Evaluation of a Possible Pre-Clovis Occupation (38AL23) Megan King [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Archaeological Anthropology Commons Recommended Citation King, Megan, "The Distribution of Paleoindian Debitage from the Pliestocene Terrace at the Topper Site: An Evaluation of a Possible Pre-Clovis Occupation (38AL23). " Master's Thesis, University of Tennessee, 2012. https://trace.tennessee.edu/utk_gradthes/1174 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Megan King entitled "The Distribution of Paleoindian Debitage from the Pliestocene Terrace at the Topper Site: An Evaluation of a Possible Pre-Clovis Occupation (38AL23)." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Master of Arts, with a major in Anthropology. Dr. David G. Anderson, Major Professor We have read this thesis and recommend its acceptance: Dr. Boyce N. Driskell, Dr. Kandace Hollenbach Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) To the Graduate Council, I am submitting herewith a thesis written by Megan M.